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Tree line dynamics in the tropical A frican highlands – identifying drivers and dynamics
Author(s) -
Jacob Miro,
Annys Sofie,
Frankl Amaury,
De Ridder Maaike,
Beeckman Hans,
Guyassa Etefa,
Nyssen Jan
Publication year - 2015
Publication title -
journal of vegetation science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.1
H-Index - 115
eISSN - 1654-1103
pISSN - 1100-9233
DOI - 10.1111/jvs.12215
Subject(s) - tree line , climate change , tropical savanna climate , deforestation (computer science) , tropics , tropical vegetation , geography , environmental science , ecosystem , ecology , agroforestry , climatology , geology , biology , computer science , programming language
Questions What are the potential drivers of tree line change in the tropical A frican highlands? Are the temperature‐sensitive tree lines in these highlands shifting as a result of climate change? Significance The high‐altitude forests provide important ecosystem services for the vulnerable environment of the tropical highlands. Climate change is expected to have pronounced effects on the tree line limit of these forests. Afro‐alpine tropical tree lines are therefore potentially valuable as a proxy of climate change and the related response of ecosystems in the tropical highlands. Location Tropical A frican highlands. Results The influence of climatic factors in the A frican tropical highlands is significantly different compared to other regions. The potentially determining factors for tree line distribution in tropical A frica are temperature, precipitation and cloudiness, carbon balance, fire and anthropo‐zoogenic impacts. Despite recent temperature increase, tree lines have not risen to higher altitudes in the tropical A frican highlands. Instead, high human pressure has caused stabilization and even recession of the tree lines below their natural climatic limit, particularly through livestock herding. But, even neglecting human pressure, there might be a lag in response time between temperature and tree line change. Conclusions The actual drivers of tree line change in the A frican tropical highlands are mainly fire and anthropogenic pressure rather than climate change. But long‐term drought periods can be a trigger for fire‐induced deforestation of the tree line vegetation. Additionally, in volcanic active mountains, volcanic activity is also a potentially limiting factor for the tree line distribution. Tree line dynamics can thus not be used as a proxy of climate change for the A frican tropical highlands.

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